SHI Builders West Orange NJ Prelim GI SWM Report 1

Yalesville-Boonton-Holyoke complex, zero to eight percent slopes (YaobBc): The Yalesville- Boonton-Holyoke complex is mapped underlying the central portion of the site. The parent material reported as loamy basaltic till deposits. The typical soil profile (as detailed in the survey) consists of decomposed plant material to one inch; loam to a depth of five inches; sandy loam to a depth of 32 inches; underlain by bedrock to a depth of 80 inches below the natural ground surface (limit of report). The depth to the water table is reported to be more than 80 inches below the natural ground surface (limit of report). Yalesville-Holyoke complex, 35 to 60 percent slopes (YaohEh): The Yalesville-Holyoke complex is mapped underlying a small area within the eastern portion of the overall site and has a similar soil profile (as detailed in the survey) to YaobBc as detail above. Haledon silt loam, zero to eight percent slopes (HanBc): The Haledon silt loam is mapped underlying the central and western portions of the site. The parent material reported as loamy basaltic till deposits. The typical soil profile (as detailed in the survey) consists of decomposed plant material to two inches; silt loam to a depth of 22 inches; loam to a depth of 30 inches; underlain by sandy loam to a depth of 80 inches below the natural ground surface (limit of report). The depth to the water table is reported to be seven to 18 inches below the natural ground surface (limit of report). Boonton-Urban land complex, zero to eight percent slopes (BowrB): The Boonton-Urban Land complex is mapped underlying the eastern portion of the site. The parent material reported as loamy sandstone and shale till deposits. The typical soil profile (as detailed in the survey) consists of decomposed plant material to one inch; silt loam to a depth of three inches; loam to a depth of 27 inches; underlain by sandy loam to a depth of 83 inches below the natural ground surface (limit of report). The depth to the water table is reported to be more than 80 inches below the natural ground surface (limit of report). Boonton-loam, eight to fifteen percent slopes (BogCc): The Boonton Loam is mapped underlying the western portion of the site. The parent material reported as loamy basaltic till deposits. The typical soil profile (as detailed in the survey) consists of decomposed plant

am is mapped underlying the western portion of the site. The parent material reported as loamy basaltic till deposits. The typical soil profile (as detailed in the survey) consists of decomposed plant material to three inches; loam to a depth of five inches; silt loam to a depth of 30 inches; sandy loam to a depth of 47 inches; underlain by loamy sand to a depth of 72 inches below the natural ground surface (limit of report). The depth to the water table is reported to be more than 80 inches below the natural ground surface (limit of report). Urban land, Boonton substratum, zero to eight percent slopes (USBONB): The Urban Land Boonton substratum is mapped underlying the northern portion of the site. The parent material reported as supraglacial till. The typical soil profile (as detailed in the survey) consists of material SHI Builders 5 4266-99-001E